Hostname: page-component-78c5997874-t5tsf Total loading time: 0 Render date: 2024-11-04T18:40:51.923Z Has data issue: false hasContentIssue false

Reply to: “Comment on ‘High Resolution Paleotemperature Proxy Record for the Last Interglaciation Based on Norwegian Speleothems’ ” by Isaac Winograd and Kenneth Ludwig

Published online by Cambridge University Press:  20 January 2017

Stein-Erik Lauritzen*
Affiliation:
Department of Geology, Bergen University, Allgaten 41, N-5007, Bergen, Norway

Abstract

Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Letter to the Editor
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Gordon, D. Smart, P. L. Ford, D. C. Andrews, J. N. Atkinson, T. C. Rowe, P. J., and Christopher, N. S. J. (1989). Dating of late Pleistocene interglacial and interstadial periods in the United Kingdom from speleothem growth frequency. Quaternary Research 31 , 1426.Google Scholar
Lauritzen, S. E. (1995). High-resolution paleotemperature proxy record during the last interglaciation in Norway from speleothems. Quaternary Research 43 , 133146.Google Scholar
Mangerud, J. (1989). Correlation of the Eemian and the Weichselian with deep sea oxygen isotope stratigraphy. Quaternary International 3/4, 14.Google Scholar
Winograd, I. J. Coplen, T. B. Landwehr, J. M. Riggs, A. C. Ludwig, K. R. Szabo, B. Kolesar, P. T., and Revesz, K. M. (1992). Continuous 500,000- Year climate record from vein calcite in Devils Hole, Nevada. Science 258 , 255260.Google Scholar